ISSN: 1003-6326
CN: 43-1239/TG
CODEN: TNMCEW

Vol. 31    No. 10    October 2021

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Sources of rare earth elements REE+Y (REY) in Bayili Coal Mine from Wensu County of Xinjiang, China
Jian-qiang XUE1,2, Jian-xin LIU1,2, De-zhi HUANG1,2, Wei-jian ZHOU1,2, Chun-ming LIU1,2, Yu-sen CAO1,2, Chuang-hua CAO1,3
(1. School of Geosciences and Info-physics, Central South University, Changsha 410083, China;
2. Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha 410083, China;
3. Hunan Institute of Geology Survey, Changsha 410011, China
)
Abstract: By analyses on the trace elements of coals, host-rocks and wall-rocks, this study aims to trace the sources and evaluate the utilization prospects of REE+Y (REY) in coals from Bayili Coal Mine (Wensu, Xinjiang, China). The distribution patterns of REY in the coals are divided into two groups, flat-type and heavy REE-enrichment type (H-type). The REY of the former was mainly from the gneisses of the basement of the coal-bearing basin, and that of the later was partly from hydrothermal solution. The host-rocks show two types of REY patterns, middle REE-enrichment type (M-type) and H-type, which are due to the injection of REY from acid terrestrial water and hydrothermal solution, respectively. Almost all the coal samples are plotted into the promising area on the diagram of percentage of critical elements (REYdef, rel) vs ratio of sum of critical elements to the sum of excessive elements (Coutl) and half of the coal samples have high contents of Ga closing to the cut-off grade of Ga deposit as by-product, which indicate that the REY and Ga in Bayili Coal Mine are of utilization prospects as by-product.
Key words: source; rare earth elements; distribution pattern; coal; Wensu County (Xinjiang)
Superintended by The China Association for Science and Technology (CAST)
Sponsored by The Nonferrous Metals Society of China (NFSOC)
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